<?xml version="1.0" encoding="UTF-8"?><article article-type="normal" xml:lang="en">
   <front>
      <journal-meta>
         <journal-id journal-id-type="publisher-id">PALEVO</journal-id>
         <issn>1631-0683</issn>
         <publisher>
            <publisher-name>Elsevier</publisher-name>
         </publisher>
      </journal-meta>
      <article-meta>
         <article-id pub-id-type="pii">S1631-0683(09)00096-7</article-id>
         <article-id pub-id-type="doi">10.1016/j.crpv.2008.11.009</article-id>
         <article-categories>
            <subj-group subj-group-type="type">
               <subject>Research article</subject>
            </subj-group>
            <subj-group subj-group-type="heading">
               <subject>Evolution (Biogenesis)</subject>
            </subj-group>
         </article-categories>
         <title-group>
            <article-title>Chemical synthesis of biomimetic forms</article-title>
            <trans-title-group xml:lang="fr">
               <trans-title>Synthèse chimique de formes biomimétiques</trans-title>
            </trans-title-group>
         </title-group>
         <contrib-group content-type="editors">
            <contrib contrib-type="editor">
               <name>
                  <surname>Gargaud</surname>
                  <given-names>Muriel</given-names>
               </name>
               <email/>
            </contrib>
            <contrib contrib-type="editor">
               <name>
                  <surname>Mustin</surname>
                  <given-names>Chistian</given-names>
               </name>
               <email/>
            </contrib>
            <contrib contrib-type="editor">
               <name>
                  <surname>Reisse</surname>
                  <given-names>Jacques</given-names>
               </name>
               <email/>
            </contrib>
         </contrib-group>
         <contrib-group content-type="authors">
            <contrib contrib-type="author">
               <name>
                  <surname>Livage</surname>
                  <given-names>Jacques</given-names>
               </name>
               <email>jacques.livage@upmc.fr</email>
            </contrib>
            <aff-alternatives>
               <aff> Chimie de la matière condensée, Collège de France, 11, place Marcelin-Berthelot, 75231 Paris, France</aff>
            </aff-alternatives>
         </contrib-group>
         <pub-date-not-available/>
         <volume>8</volume>
         <issue seq="4">7</issue>
         <issue-id pub-id-type="pii">S1631-0683(09)X0007-2</issue-id>
         <issue-title>Traces de vie présente ou passé: quels indices, signatures ou marqueurs?</issue-title>
         <issue-title xml:lang="en">Traces of past or present life: biosignatures and potential life indicators?</issue-title>
         <fpage seq="0" content-type="normal">629</fpage>
         <lpage content-type="normal">636</lpage>
         <history>
            <date date-type="received" iso-8601-date="2008-06-02"/>
            <date date-type="accepted" iso-8601-date="2008-11-12"/>
         </history>
         <permissions>
            <copyright-statement>© 2009 Académie des sciences. Published by Elsevier B.V. All rights reserved.</copyright-statement>
            <copyright-year>2009</copyright-year>
            <copyright-holder>Académie des sciences</copyright-holder>
         </permissions>
         <self-uri xmlns:xlink="http://www.w3.org/1999/xlink" content-type="application/pdf" xlink:href="main.pdf">
                        Full (PDF)
                    </self-uri>
         <abstract abstract-type="author">
            <p>The biogenic origin of the first traces of life is often based on the morphological analysis of microfossils. However life-like forms can also be obtained via chemical synthesis from purely inorganic precursors. Many examples can be found in literature that are mainly based on aqueous solution chemistry. Osmotic growth of gelatinous precipitates is observed during the formation of “chemical gardens”. Point defects in surfactant mesophases lead to mesoporous silica with curved shapes. The oriented attachment of nanocrystals via hydrophilic polymers leads to mesocrystals that exhibit a large variety of unusual shapes.</p>
         </abstract>
         <trans-abstract abstract-type="author" xml:lang="fr">
            <p>L’origine biogénique des premières traces fossiles est souvent basée sur une analyse morphologique. Il apparaît toutefois que des formes analogues peuvent être obtenues par synthèse chimique, à partir d’éléments purement minéraux. De nombreux exemples sont décrits dans la littérature, qui font intervenir le plus souvent la chimie des solutions aqueuses. Les processus de croissance osmotique de précipités gélatineux sont à l’origine de la formation des « jardins chimiques ». La présence de défauts ponctuels dans les mésophases de surfactants conduit à des silices mésoporeuses qui présentent des surfaces courbes. L’association contrôlée de nanocristaux via des polymères hydrophiles provoque la croissance de mésocristaux qui présentent des formes inhabituelles.</p>
         </trans-abstract>
         <kwd-group>
            <unstructured-kwd-group>Mesocrystals, Biomorph silica, Chemical garden</unstructured-kwd-group>
         </kwd-group>
         <kwd-group xml:lang="fr">
            <unstructured-kwd-group>Mésocristaux, Silice biomorphe, Jardin chimique</unstructured-kwd-group>
         </kwd-group>
         <custom-meta-group>
            <custom-meta>
               <meta-name>presented</meta-name>
               <meta-value>Written on invitation of the Editorial Board</meta-value>
            </custom-meta>
         </custom-meta-group>
      </article-meta>
   </front>
   <body>
      <sec>
         <label>1</label>
         <title>Introduction</title>
         <p>Fossilized remains have been studied for centuries and the search for the first traces of life has long been based on the shape of microfossils. Organic matter usually degrades quite fast so that only hard parts of a body (bones, shells, teeth…) or mineralized tissue can be found as fossils. New analytical technologies have been applied to fossil materials during the past decade in order to confim their biogenic origin <xref rid="bib32" ref-type="bibr">[32]</xref>, but morphology is still one of the main parameters to decide whether microfossils could be considered as traces of life rather than just mineral forms.</p>
         <p>Minerals usually exhibit regular crystalline shapes, while living organisms build much more sophisticated architectures. This can be easily illustrated by comparing quartz crystals with the shells of diatoms. Both are made of silica (SiO<sub>2</sub>) but their shape is completely different. A similar comparison could also been made with calcium carbonate (CaCO<sub>3</sub>), between aragonite crystals and coccolithe shells. These examples suggest that it should be quite straightforward to decide whether fossil traces are from biogenic origin. There is no doubt either about the biological nature of dinosaur bones or ammonite shells buried in ancient sediments. However, this is no longer the case when microorganisms such as bacteria are involved. Microfossils coming from the most ancient forms of life on Earth are often difficult to recognize and controversies based on the analysis of shapes can be often found in literature.</p>
         <p>The biogenicity of most structures previously interpreted as Archean microfossils has been often questioned <xref rid="bib35" ref-type="bibr">[35]</xref>. The controversy arises from the fact that natural abiotic processes have been shown to be able to lead to biological morphology. This can be well illustrated by the debate about the microbe-like filaments found in the Precambrian Warrawoona chert formation in western Australia. Schopf et al. reported that these were the earliest traces of life on Earth, due to cyanobateria about 3500 billion years old <xref rid="bib31" ref-type="bibr">[31]</xref>. But, in the same issue of <italic>Nature</italic>, Brasier et al. showed that similar shapes could be formed from inorganic precursors under hydrothermal conditions <xref rid="bib2" ref-type="bibr">[2]</xref> and a year later, Garcia-Ruiz et al. synthesized micron-sized silica-coated carbonate filaments exhibiting curved helical morphologies, reminiscent of biological forms. They were made upon heating BaCl<sub>2</sub> in alkaline sodium silicate solutions <xref rid="bib12" ref-type="bibr">[12]</xref>. Self-assembled silica-carbonate aggregates have been obtained that exhibit strong resemblance to biogenic forms <xref rid="bib15" ref-type="bibr">[15]</xref>. As pointed out by these authors, morphology should be considered as an ambiguous indicator of biogenicity <xref rid="bib11" ref-type="bibr">[11]</xref> and <xref rid="bib23" ref-type="bibr">[23]</xref> (<xref rid="fig1" ref-type="fig">Fig. 1</xref>).</p>
         <p>The following question then arises. Is it possible via chemical morphogenesis to synthesize shapes usually typical of life? The synthesis of complex form by living organisms is a real challenge for chemists <xref rid="bib24" ref-type="bibr">[24]</xref> and reproducing the forms of life has long been a dream for all chemists <xref rid="bib34" ref-type="bibr">[34]</xref>! This article describes some examples of inorganic syntheses leading to the formation of biomorph solids.</p>
      </sec>
      <sec>
         <label>2</label>
         <title>Chemical gardens</title>
         <sec>
            <p>One of the first chemical syntheses of living forms was reported about a century ago by Stephane Leduc. He showed that a spectacular plant-like growth occurs when crystals of metal salts (FeCl<sub>3</sub>, CuSO<sub>4</sub>, Ni(NO<sub>3</sub>)<sub>2</sub>, CoCl<sub>2</sub>) are dropped into an aqueous solution of sodium silicate (water glass) <xref rid="bib4" ref-type="bibr">[4]</xref>. Colorful plant-like extensions grow from the surface of each crystal giving rise to the so-called “chemical gardens” (<xref rid="fig2" ref-type="fig">Fig. 2</xref>). At that time Stephane Leduc thought he was able to create some artificial life leading to the publication of many papers about the mechanism of life <xref rid="bib19" ref-type="bibr">[19]</xref> and <xref rid="bib20" ref-type="bibr">[20]</xref>!</p>
         </sec>
         <sec>
            <p>Two physicochemical processes are actualy involved in the formation of these chemical gardens.</p>
         </sec>
         <sec>
            <label>2.1</label>
            <title>Precipitation of oxides or hydroxides from aqueous solutions of metal salts</title>
            <sec>
               <p>The first one is the precipitation of oxides or hydroxides from aqueous solutions of metal salts. This process is mainly governed by the pH of the solution.</p>
            </sec>
            <sec>
               <p>When dissolved in water, salts of low-valent metal cations (Cu<sup>2+</sup>, Co<sup>2+</sup>, Fe<sup>3+</sup>…) give acid solutions in which metal cations are solvated by dipolar water molecules. Precipitation occurs by adding a base in order to increase the pH.<disp-formula>
                     <alternatives/>
                  </disp-formula>
               </p>
            </sec>
            <sec>
               <p>The reverse is observed for silica which is only soluble in an alkaline medium. The precipitation of silica from a silicate solution occurs by adding an acid to decrease the pH.<disp-formula>
                     <alternatives/>
                  </disp-formula>
               </p>
            </sec>
            <sec>
               <p>When a crystal of an acid metal salt is dropped into an alkaline silicate solution, the salt progressively dissolves and a strong pH gradient is formed between the acid solution surrounding the crystal and the basic silicate solution. Precipitation then occurs at the interface between both solutions.</p>
            </sec>
         </sec>
         <sec>
            <label>2.2</label>
            <title>Osmotic growth</title>
            <sec>
               <p>The second process is called osmotic growth.</p>
            </sec>
            <sec>
               <p>Actually a gelatinous precipitate of hydrous silicate is formed that behaves as a semi-permeable membrane <xref rid="bib28" ref-type="bibr">[28]</xref>. The acid solution inside the membrane is much more concentrated than the basic silicate solution outside. An osmotic pressure is then established between both sides of the gelatinous precipitate inducing water diffusion through the membrane inward. The crystal continues to dissolve and the membrane to swell until it breaks. Some concentrated salt acid solution is then ejected into the basic silicate medium and a new precipitate immediately forms. Tubular fibres then develop from each point of rupture giving rise to the spectacular plant-like shape of the chemical gardens <xref rid="bib1" ref-type="bibr">[1]</xref>.</p>
            </sec>
            <sec>
               <p>The physicochemical parameters leading to the formation of chemical gardens have been studied using more sophisticated analytical methods during the past decade in order to get a better understanding of this amazing reaction. NMR and ESCA experiments for instance show that aluminosilicates rather than hydroxides are formed with Al(NO<sub>3</sub>)<sub>3</sub> crystals <xref rid="bib10" ref-type="bibr">[10]</xref>. Hollow fibres actually grow from the crystal <xref rid="bib27" ref-type="bibr">[27]</xref>. Bubbles are formed at the tip of these fibres guiding their tubular growth <xref rid="bib36" ref-type="bibr">[36]</xref> and <xref rid="bib37" ref-type="bibr">[37]</xref>. Gravity appears also to be involved so that chemical gardens have been grown in space <xref rid="bib16" ref-type="bibr">[16]</xref>.</p>
            </sec>
         </sec>
      </sec>
      <sec>
         <label>3</label>
         <title>Biomorph mesoporous silica</title>
         <sec>
            <p>Biogenic silica has been used by planktonic microorganisms for their protection. Diatoms provide a wondeful example of the beautiful architectures made by life. These single-cell microalgeas are surrounded by a porous silica shell (frustule) that exhibits an increadible variety of shapes. Chemists are very interested by these microorganisms that are able to make silica glasses under ambiant conditions while high temperatures are required to make industrial glasses from molten silica. Therefore the soft solution synthesis of porous silica glasses is becoming a very popular field of research. It leads to the development of the so-called sol–gel process <xref rid="bib3" ref-type="bibr">[3]</xref>. Sol–gel silica is made via the hydrolysis and condensation of molecular precursors such as silicon alkoxides Si(OR)<sub>4</sub> (R<private-char name="dbnd">
                  <glyph-data/>
               </private-char>CH<sub>3</sub>, C<sub>2</sub>H<sub>5</sub>…) as follows:<disp-formula>
                  <alternatives/>
               </disp-formula>
               <disp-formula>
                  <alternatives/>
               </disp-formula>
            </p>
         </sec>
         <sec>
            <p>An hydrous silica gel is formed that transforms into a silica glass upon heating. One of the main advantages of the sol–gel route is to allow the powderless processing of glasses and ceramics. It has been widely developped for the production of fibres and coatings <xref rid="bib17" ref-type="bibr">[17]</xref>.</p>
         </sec>
         <sec>
            <p>The sol–gel route leads to the formation of porous silica gels, but their pore size cannot be accurately controlled. A real breakthrough occurred when scientists at Mobil showed that it was possible to get ordered mesoporous silica in the presence of surfactants such as cethyltrimethylammonium chloride (CTACl) <xref rid="bib18" ref-type="bibr">[18]</xref>.</p>
         </sec>
         <sec>
            <p>Surfactant molecules are made of a long hydrophobic alkyl tail and a polar hydrophilic head. They self-assemble in polar solvents such as water to give micelles in which all polar heads are directed toward the outside aqueous medium. Mesophases are formed when surfactants are mixed with oil and water. Mesoporous silica is then obtained via a “liquid crystal templating” process. Depending on concentration, different mesophases (hexagonal, cubic, lamellar) are obtained that behave as templates for the synthesis of porous silica. Molecular precursors, alkoxides Si(OR)<sub>4</sub> or silicic acid Si(OH)<sub>4</sub> occupy the continuous water region. Condensation leads to the formation of silica walls between the surfactants assemblies. Organic surfactants are removed via calcination leaving a porous silica network. A periodic mesoporous structure can then be obtained leading to the development of mesoporous silicas which are nowadays extensively used in the field of catalysis.</p>
         </sec>
         <sec>
            <p>Chemists are usually looking for defect free mesoporous structures. However, it is well known that topological defects, points, lines or planes can be observed during the formation of surfactant mesophases. The energy required to stabilize these defects is much smaller than in solid crystals. Large defects several micrometers in dimensions can be easily formed. The condensation of silica around these defects leads to curved shapes so that the resulting solid particles exhibit sophisticated curves that look like biogenic silica (<xref rid="fig3" ref-type="fig">Fig. 3</xref>) <xref rid="bib13" ref-type="bibr">[13]</xref> and <xref rid="bib14" ref-type="bibr">[14]</xref>.</p>
         </sec>
         <sec>
            <p>Hexagonal mesoporous silicas, MCM-41, have been extensively studied by Ozin. They are built of assemblies of rod-like 2D hexagonal array of surfactants. Topological point defects change the orientation of the director field leading to the formation of curved structures that can initiate and direct the growth of particular forms of mesoporous silica: discoidal, toroidal, disk-like, spiral, spheroidal <xref rid="bib25" ref-type="bibr">[25]</xref>. The condensation of silica mainly quenches the topological defect and its associated director field pattern. It is possible to draw a relation between a specific type of defect and a particular mesoporous silica shape <xref rid="bib26" ref-type="bibr">[26]</xref>. Each morphology can be associated with a specific kind of dislocation or disclination defect (<xref rid="fig4" ref-type="fig">Fig. 4</xref>). Two defects can even combine to lead to more spohisticated morphologies (bagel, twisted toroid…).</p>
         </sec>
      </sec>
      <sec>
         <label>4</label>
         <title>Crystal tectonics and mesocrystals</title>
         <sec>
            <p>Biomorph shapes have been mainly obtained with silica-based materials. Silica is a well known glass former that leads to amorphous solids. Curved surfaces are then much easier to form in the absence of crystallographic constraints. This is no longer the case when crystals are used as precursors. Flat surfaces corresponding to the crystallographic planes, with definite angles, are then usually observed. Curved surfaces could anyway be obtained via the controlled self-assembly of nanocrystals, leading to ordered superstructures called “mesocrystals” <xref rid="bib8" ref-type="bibr">[8]</xref> and <xref rid="bib9" ref-type="bibr">[9]</xref>.</p>
         </sec>
         <sec>
            <p>These mesocrystals somehow mimic the formation of biostructures found in the hammer-shaped building units of coccoliths or the skeletal plates of sea urchins.</p>
         </sec>
         <sec>
            <p>Mesocrystals are formed via a bottom-up process that couples together chemical synthesis and self-assembly in order to produce complex superstructures. Syntheses are performed in the presence of organic additives that limit crystal growth and control their aggregation. Self-organization leads to single-crystalline structures with included organic additives as defects. Mesocrystals could be considered as a special case of colloidal crystals in which building units are anistropic nanocrystals rather than spherical colloidal particles. They could be described as “crystals of crystals” in which the building units are nanocrystals rather than ions or molecules.</p>
         </sec>
         <sec>
            <p>The formation of mesocrystals is a two-step reaction in which organic additives play a double role (<xref rid="fig5" ref-type="fig">Fig. 5</xref>):<list>
                  <list-item>
                     <label>•</label>
                     <p>in the first step, organic additives bind to some crystalline faces. Crystal growth is then limited leading to the formation of nanocrystals stabilized by the organic molecules adsorbed at their surface;</p>
                  </list-item>
                  <list-item>
                     <label>•</label>
                     <p>in the second step, weak interactions between organic additives favor the controlled aggregation of the nanocrystalline building blocks, leading to ordered superstructures.</p>
                  </list-item>
               </list>
            </p>
         </sec>
         <sec>
            <p>The synthesis of BaSO<sub>4</sub> (or CrO<sub>4</sub>) mesocrystals provides a nice example of such a process. Linear chains of prismatic nanoparticles have been synthesized from a mixture of baryum sulfosuccinate reverse micelles and sodium sulfosuccinate microemulsions containing encapsulated sulfate or chromate anions. Slow exchange between these two components leads to the formation of BaSO<sub>4</sub> or BaCrO<sub>4</sub> nanoparticles <xref rid="bib21" ref-type="bibr">[21]</xref>. The anionic groups (SO<sub>4</sub>)<sup>2–</sup> or (CrO<sub>4</sub>)<sup>2–</sup> preferentially bind to some faces of the crystals leading to the formation of prismatic nanoparticles. Interactions between organic chains of the surfactants then lead to the directed aggregation along the axis perpendicular to the larger faces in order to maximize the hydrophobic interactions. Nanocrystals within a chain are separated by a regular spacing of 2 nm corresponding to an interdigitated bilayer of surfactant molecules (<xref rid="fig6" ref-type="fig">Fig. 6</xref>).</p>
         </sec>
         <sec>
            <p>Double hydrophilic block copolymers (DHBC) have been recently introduced to control the formation of mesocrystals <xref rid="bib6" ref-type="bibr">[6]</xref> and <xref rid="bib22" ref-type="bibr">[22]</xref>. They are made of two hydrophilic blocks. One is strongly interacting with the inorganic particles while the other one does not. In the PEG-b-PMAA block copolymer for instance, the carboxylic groups of the PolyMethAcrylic Acid (PMAA) strongly interacts with the inorganic particles while Polythylene Glycol (PEG) only provides solubility.</p>
         </sec>
         <sec>
            <p>Complex morphologies have been obtained via the precipitation of BaSO<sub>4</sub> (or BaCrO<sub>4</sub>) in the presence of the PEG-b-PMAA–PO<sub>3</sub>H<sub>2</sub> block copolymer (<xref rid="fig7" ref-type="fig">Fig. 7</xref>) <xref rid="bib33" ref-type="bibr">[33]</xref>.</p>
         </sec>
         <sec>
            <p>The complexing power of DHBC depends on the nature of the functional groups (–COOH, –PO<sub>3</sub>H<sub>2</sub>, –SO<sub>3</sub>H) and their protonation state, i.e. on pH. A large variety of forms can be obtained <xref rid="bib7" ref-type="bibr">[7]</xref> and <xref rid="bib8" ref-type="bibr">[8]</xref>. Bundles of coiled single-crystalline BaSO<sub>4</sub> nanofilamnents are obtained in the presence of poly(ethylene oxide)-<italic>block</italic>-poly(methacrylic acid) (PEO-<italic>b</italic>-PMAA–PO<sub>3</sub>H<sub>2</sub>) <xref rid="bib29" ref-type="bibr">[29]</xref> and <xref rid="bib30" ref-type="bibr">[30]</xref>.</p>
         </sec>
      </sec>
      <sec>
         <label>5</label>
         <title>Conclusion</title>
         <sec>
            <p>Only a few examples have been described in this article. They show that chemical morphogenesis can lead to sophisticated structures. Preparing man-made materials with life-like forms becomes nowadays quite fashionable <xref rid="bib23" ref-type="bibr">[23]</xref>. However, this is not the only aim of these research works. Shape is also very important for materials scientists. The properties of a given material often depend on its shape. Glass windows or fibres for instance are used for their transparency. Glass wool is used for its insulating properties and glass bottles as containers. Moreover, the development of nanotechnologies requires the synthesis of nanostructured materials. In this field, bio-materials provide a nice guide for the synthesis of bio-inspired materials.</p>
         </sec>
      </sec>
   </body>
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                  <given-names>O.</given-names>
               </name>
               <article-title>Bubble guidance of tubular growth in reaction–precipitation systems</article-title>
               <source>Phys. Chem. Chem. Phys.</source>
               <volume>7</volume>
               <year>2005</year>
               <page-range>2610–2615</page-range>
            </element-citation>
         </ref>
      </ref-list>
   </back>
   <floats-group>
      <fig id="fig1">
         <label>Fig. 1</label>
         <caption>
            <p>Self-assembled nanocrystals obtained via chemical synthesis from inorganic precursors. a, b: silica–witherite (SiO<sub>2</sub>–BaCO<sub>3</sub>) biomorphs (from <xref rid="bib7" ref-type="bibr">[7]</xref>); c: BaCO<sub>3</sub> helices induced by racemic block copolymers (from <xref rid="bib8" ref-type="bibr">[8]</xref>).</p>
            <p>Fig. 1. Auto-organisation de nanocristaux obtenus par synthèse chimique à partir de précurseurs inorganiques. a, b : biomorphes silice–witherite (SiO<sub>2</sub>–BaCO<sub>3</sub>) (d’après <xref rid="bib7" ref-type="bibr">[7]</xref>) ; c : hélices de BaCO<sub>3</sub> obtenues en présence de copolymères blocs racémiques.</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr1.jpg"/>
      </fig>
      <fig id="fig2">
         <label>Fig. 2</label>
         <caption>
            <p>Chemical gardens obtained by diping CoCl<sub>2</sub> crystals in a silicate solution (photo from Stéphane Querbes, for “les atomes crochus” and “Animascience”).</p>
            <p>Fig. 2. Jardin chimique obtenu en plongeant des cristaux de CoCl<sub>2</sub> dans une solution de silicate (photo de Stéphane Querbes pour « les atomes crochus » et « animascience »).</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr2.jpg"/>
      </fig>
      <fig id="fig3">
         <label>Fig. 3</label>
         <caption>
            <p>Biomorph silica (from <xref rid="bib5" ref-type="bibr">[5]</xref>).</p>
            <p>Fig. 3. Silices biomorphes (d’après <xref rid="bib5" ref-type="bibr">[5]</xref>).</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr3.jpg"/>
      </fig>
      <fig id="fig4">
         <label>Fig. 4</label>
         <caption>
            <p>The role of defects in the formation of mesoporous silica (from <xref rid="bib26" ref-type="bibr">[26]</xref> and <xref rid="bib27" ref-type="bibr">[27]</xref>).</p>
            <p>Fig. 4. Rôle des défauts dans la formation de silices mésoporeuses (d’après <xref rid="bib26" ref-type="bibr">[26]</xref> and <xref rid="bib27" ref-type="bibr">[27]</xref>).</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr4.jpg"/>
      </fig>
      <fig id="fig5">
         <label>Fig. 5</label>
         <caption>
            <p>Formation of mesocrystals in the presence of organic additives.</p>
            <p>Fig. 5. Rôle des additifs organiques dans la formation des mésocristaux.</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr5.jpg"/>
      </fig>
      <fig id="fig6">
         <label>Fig. 6</label>
         <caption>
            <p>Ordered chains of prismatic BaCrO<sub>4</sub> particles prepared in AOT microemulsions (from <xref rid="bib30" ref-type="bibr">[30]</xref>).</p>
            <p>Fig. 6. Formation de chaînes de particules prismatiques de BaCrO<sub>4</sub> au sein de microémulsions (d’après <xref rid="bib30" ref-type="bibr">[30]</xref>).</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr6.jpg"/>
      </fig>
      <fig id="fig7">
         <label>Fig. 7</label>
         <caption>
            <p>Some examples of BaSO<sub>4</sub> mesocrystals prepared in the presence of double hydrophilic block copolymers (from <xref rid="bib31" ref-type="bibr">[31]</xref>, <xref rid="bib32" ref-type="bibr">[32]</xref>, <xref rid="bib35" ref-type="bibr">[35]</xref>, <xref rid="bib36" ref-type="bibr">[36]</xref> and <xref rid="bib37" ref-type="bibr">[37]</xref>). Some examples of BaSO<sub>4</sub> mesocrystals grown in the presence of block copolymers. a: PEO-<italic>b</italic>-PEI–SO<sub>3</sub>H (from ref. <xref rid="bib7" ref-type="bibr">[7]</xref>); b: PEO-b-PMAA–PO<sub>3</sub>H<sub>2</sub> (from ref. <xref rid="bib22" ref-type="bibr">[22]</xref>); c: BaSO<sub>4</sub> fiber bundles with PEO-b-PMAA–PO<sub>3</sub>H<sub>2</sub> (from ref. <xref rid="bib29" ref-type="bibr">[29]</xref>); d: cone-shaped BaSO<sub>4</sub> particles with polyacrylate (from ref. <xref rid="bib29" ref-type="bibr">[29]</xref>).</p>
            <p>Fig. 7. Exemples de mésocristaux de BaSO<sub>4</sub> formés en présence de copolymères blocs hydrophiles (d’après <xref rid="bib31" ref-type="bibr">[31]</xref>, <xref rid="bib32" ref-type="bibr">[32]</xref>, <xref rid="bib35" ref-type="bibr">[35]</xref>, <xref rid="bib36" ref-type="bibr">[36]</xref> and <xref rid="bib37" ref-type="bibr">[37]</xref>).</p>
         </caption>
         <graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="main.assets/gr7.jpg"/>
      </fig>
   </floats-group>
</article>